Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert

doi:10.7522/j.issn.1000-694X.2015.00025

JOURNAL OF DESERT RESEARCH ›› 2016, Vol. 36 ›› Issue (3): 798-804.DOI: 10.7522/j.issn.1000-694X.2015.00025

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Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert

Wei Yaping^1,2, Fan Jinglong¹, Xu Xinwen¹, Jin Xiaojun³, Zhou Hongwei³

1. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. PetroChina Tarim Oilfield Company, Korla 841000, Xinjiang, China

Received:2014-11-21 Revised:2015-02-06 Online:2016-05-20 Published:2016-05-20

Abstract

Abstract:

The oil and natural gas resources are rich in the hinterland of the Taklamakan desert, where weather is extremely dry, ecological environment is extremely frail. In this study,in order to provide dependable foundation for the reasonable exploitation of groundwater, the protection and improvement of water quality. A section crossing the from Kunlun piedmont to the hinterland of Taklimakan Desert is monitored,Piper diagram is utilized to analyze the hydrochemical type, and NETPATH Modeling is used to simulate the process of chemical evolution of groundwater. The results obtained are stated as follows: (1) The groundwater hydrochemical types are comparatively single in the area, the main types are Na-Mg-Cl-SO₄ and Na-Cl-SO₄; (2) The main representation properties of the water chemical evolution model are the strong evaporation and concentration, the dissolution of mirabilite, rock salt and pyroxene, and the more prominent Ca²⁺/Na⁺ ion exchange.

Key words: groundwater, chemical evolution, NETPATH model, Taklimakan Desert

CLC Number:

P641.12

Wei Yaping, Fan Jinglong, Xu Xinwen, Jin Xiaojun, Zhou Hongwei. Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert[J]. JOURNAL OF DESERT RESEARCH, 2016, 36(3): 798-804.

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Hydrogeochemical Modelling of Groundwater Chemical Evolution fromSouthern Margin to Hinterland of the Taklamakan Desert

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